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Altocumulus clouds are a mid-altitude cloud formation characterized by large, whitish, fleecy masses with shaded portions. The name "altocumulus" comes from Latin "altus" (high) and "cumulus" (heap). These clouds are part of the broader classification of clouds, which are visible masses of water droplets or ice crystals suspended in the air. Clouds form when moist air rises, expands, and cools to its dew point, causing water vapor to condense onto tiny particles. Altocumulus clouds are classified as middle clouds, typically found at heights between 2 to 7 kilometers (1 to 4 miles). They are distinct from stratus clouds, which form flat layers, and cumulus clouds, which are puffy.1234

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